Official Series Description


Lab Data Summary

Aggregate lab data for the BAILE soil series. This aggregation is based on all pedons with a current taxon name of BAILE, and applied along 1-cm thick depth slices. Solid lines are the slice-wise median, bounded on either side by the interval defined by the slice-wise 5th and 95th percentiles. The median is the value that splits the data in half. Five percent of the data are less than the 5th percentile, and five percent of the data are greater than the 95th percentile. Values along the right hand side y-axis describe the proportion of pedon data that contribute to aggregate values at this depth. For example, a value of "90%" at 25cm means that 90% of the pedons correlated to BAILE were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.


Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BAILE soil series. Monthly precipitation (PPT) and potential evapotranspiration (PET) have been estimated from the 50th percentile of gridded values (PRISM 1981-2010) overlapping with the extent of SSURGO map units containing each series as a major component. Monthly PET values were estimated using the method of Thornthwaite (1948). These (and other) climatic parameters are calculated with each SSURGO refresh and provided by the fetchOSD function of the soilDB package. Representative water storage values (“AWC” in the figures) were derived from SSURGO by taking the 50th percentile of profile-total water storage (sum[awc_r * horizon thickness]) for each soil series. Note that this representation of “water storage” is based on the average ability of most plants to extract soil water between 15 bar (“permanent wilting point”) and 1/3 bar (“field capacity”) matric potential. Soil moisture state can be roughly interpreted as “dry” when storage is depleted, “moist” when storage is between 0mm and AWC, and “wet” when there is a surplus. Clearly there are a lot of assumptions baked into this kind of monthly water balance. This is still a work in progress.

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Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the BAILE series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

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Select annual climate data summaries for the BAILE series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

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Geomorphic description summaries for the BAILE series and siblings. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. Proportions can be interpreted as an aggregate representation of geomorphic membership. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Small Shannon entropy values suggest relatively consistent geomorphic association, while larger values suggest lack thereof. Source: SSURGO component records .

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Click the image to view it full size.

There are insufficient data to create the 3D terrace figure.

There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with BAILE share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

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Select annual climate data summaries for the BAILE series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the BAILE series and competing. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Proportions can be interpreted as an aggregate representation of geomorphic membership. Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Shannon entropy values close to 0 represent soil series with relatively consistent geomorphic association, while values close to 1 suggest lack thereof. Source: SSURGO component records .

Click the image to view it full size.

Click the image to view it full size.

There are insufficient data to create the 3D mountains figure.

There are insufficient data to create the 3D terrace figure.

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with BAILE, arranged according to family differentiae. Hovering over a series name will print full classification and a small sketch from the OSD. Source: snapshot of SC database .

Block Diagrams

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. MD-2010-09-03-02 | City of Baltimore - 1998

    Pattern of soils in the Urban land-Legore association (Soil Survey of City of Baltimore, Maryland; 1998).

  2. MD-2010-09-10-02 | Cecil County -

    Glenelg-Brinklow-Manor-Glenville association (Soil Survey of Cecil County, Maryland).

  3. MD-2010-09-10-06 | Howard County - 2008

    Relationship of soils, topography, and underlying material in the Occoquan-Brinklow-Glenelg general soil map unit (Soil Survey of Howard County, Maryland; 2008).

  4. MD-2010-09-10-08 | Howard County - 2008

    Relationship of soils, topography, and underlying material in the Glenelg-Manor-Glenville general soil map unit (Soil Survey of Howard County, Maryland; 2008).

  5. MD-2012-02-03-03 | City of Baltimore - 1998

    Pattern of soils in the Urban land-Legore association (Soil Survey of City of Baltimore, Maryland; 1998).

  6. MD-2012-02-03-06 | Baltimore County - March 1976

    Cross section showing typical soil pattern in the Chester-Glenelg association (Soil Survey of Baltimore County, Maryland; March 1976).

  7. MD-2012-02-03-22 | Montgomery County - July 1995

    Typical pattern of soils in the Piedmont physiographic province in Montgomery County (Soil Survey of Montgomery County, Maryland; July 1995).

  8. PA-2010-09-30-04 | Adams County - 2005

    Typical pattern of soils and parent material in the Glenelg-Mt. Airy general soil map unit (Soil Survey of Adams County, Pennsylvania; 2005).

  9. PA-2010-09-30-16 | York County - 2002

    Typical pattern of soils and parent material in the Chester-Glenelg general soil map unit (Soil Survey of York County, Pennsylvania; 2002).

  10. PA-2012-03-13-48 | Lancaster County - May 1985

    Typical pattern of soils and underlying material in the Manor-Chester-Glenelg unit (Soil Survey of Lancaster County, PA; 1985).

Map Units

Map units containing BAILE as a major component. Limited to 250 records.

Map Unit Name Symbol Map Unit Area (ac) Map Unit Key National Map Unit Symbol Soil Survey Area Publication Date Map Scale
Baile-Glenville complex, 0 to 8 percent slopesBbB22524798652p7hnde00320091:24000
Baile silt loam, 3 to 8 percent slopesBaB2262645487pnp5md00520101:12000
Baile silt loam, 0 to 3 percent slopesBaA100324820582p9sdmd00520101:12000
Baile-Urban land complex, 0 to 8 percent slopesBbB30924040202lpl1md00520101:12000
Baile silt loam, 3 to 8 percent slopesBaB552824939472pqrwmd01320101:12000
Baile silt loam, 0 to 3 percent slopesBaA196124939462pqrvmd01320101:12000
Baile-Glenville complex, 3 to 8 percent slopesBbB244824407172mxrtmd01520091:12000
Baile silt loam, 0 to 3 percent slopesBaA232724407162mxrsmd01520091:12000
Glenville-Baile silt loams, 3 to 8 percent slopesGuB2908534974kyp7md02120011:12000
Baile-Glenville silt loams, 0 to 8 percent slopesBcB1477534906kym1md02120011:12000
Glenville-Baile silt loams, 0 to 8 percent slopesGnB7011793003vm5rmd02720041:12000
Baile silt loam, 0 to 3 percent slopesBaA2538792298vlg0md02720041:12000
Baile silt loam, 0 to 3 percent slopes6A9240533674kxb9md03119891:15840
Baile-Urban land complex, 0 to 8 percent slopes1UB84533912kxkzmd51019931:12000
Baile silt loam, 0 to 3 percent slopesBaA832533354kwzzmd60019721:15840
Baile silt loam, 3 to 8 percent slopesBaB804533355kx00md60019721:15840
Baile silt loamBa646545554l9pjpa00119911:24000
Baile silt loamBa3612641304pjb7pa02920081:24000
Baile silt loam, 3 to 8 percent slopesBaB3035886536yrhypa02920081:24000
Baile silt loam, 0 to 8 percent slopes, very stonyBbB136616018961qrx2pa02920081:24000
Urban land-Baile complex, 0 to 8 percent slopesUrbB6316120391r3g8pa02920081:24000
Baile silt loam, frequently ponded, 0 to 3 percent slopesBaA124498453330cgnpa04519601:20000
Baile silt loam, frequently ponded, 0 to 8 percent slopes, very stonyBcB31098453730cgrpa04519601:20000
Baile silt loam, 3 to 8 percent slopesBbB2398453430cgppa04519601:20000
Baile silt loamBa1472542717l6r0pa07119821:15840
Baile silt loamBa628542808l6typa13319901:24000
Baile stony silt loam, 2 to 7 percent slopesBaB394516924kbwzva11319671:15840
Baile loam, 0 to 4 percent slopes6A1912521228khctva15319851:15840

Map of Series Extent

Approximate geographic distribution of the BAILE soil series. To learn more about how this distribution was mapped, or to compare this soil series extent to others, use the Series Extent Explorer (SEE) application. Source: generalization of SSURGO geometry .